1000 resultados para Moisio, Arto: Marin kielen sanaston kehitys 1900-luvulla


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For the first time, small mammals were found at the earliest marine level in the northeastern part of the lower Tagus basin, to the NE of Lisbon. At this new locality, at the 10 kilometer of the Lisbon-Oporto A1-IP1 highway,conglomerates yielded, along with marine fossils, more or less abraded teeth and bones from insectivores,lagomorphs, rodents and small artiodactyls (sec Tableau 1). Age may he ascribed to the lower Miocene, MN 2b Neogene mammal unit (about 22 My), but an early MN 3 age cannot be entirely excluded. That corresponds to latest Aquitanian (or less probably earliest Burdigalian) (sec Tableau 2). This is the first hitherto found locality with small mammals of this age as far as Portugal is concerned, as well as the oldest locality so far known in the Tagus basin. Km 10 is somewhat older than the localities of Universidade Católica and Avenida do Uruguay in Lisbon (ANTUNES & MEIN, 1986). Hence we can rather accurately date the age of the first marine transgression in the northeastern part of the lower Tagus basin. This shows that in this region there are no marine equivalents of the "Venus ribeiroi beds" (Aquitanian,Division 1 of the Lisbon Miocene series). Correlation between this unit and the uppermost levels of the essentially paleogene "Complexo de Benfica" may be possible. Fossils at km 10 point out to shallow, coastal, highenergy marine environments. Sedimentological features are compatible with this model. Dry land and swamps with brackish (or ev en fresh) waters were present nearby. From those areas came remains of mammals, crocodylians, as well as oysters and charophytes that were later transported to the sea. Sea was warmer than the extant Atlantic at the same latitudes, even if conditions were not strictly tropical then. These conditions surely influenced climate in the nearby regions. Ecological data concerning mammalian faunas distinctly point out to nearby forest-rich environments, much more so than for Universidade Católica and Avenida do Uruguay localities, from where drier, even steppe environment forms largely prevail.

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The Mid Miocene marine formations of Salles area (former "Sallomacian" stage) have been studied again from numerous outcrops and cores. The deep structural framework influences notably of the characteristics and distribution of the deposits, which are neritic. The stratigraphy is stated precisely thanks to the planktonic fauna and floradetailed examination (probably Serravallian zones NN6 - N12). Several paleobiofacies are reconstituted from the rich invertebrate faunas, which give also paleoclimatic data.

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Tese de Doutoramento em História Contemporânea Institucional e Política de Portugal

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Las investigaciones de historia política abarcan un campo que la sociedad visualiza como una totalidad provista de sentido y en la cual, en conflictivo proceso de elaboración de normativas de lo participable y compartible, adquiere una forma de vida de la que todos sus miembros toman parte (grupos, individuos, de arriba, de abajo, hombres y mujeres, etc.) En esa construcción continua está la génesis de los problemas contemporáneos, y en el diálogo permanente entre pasado y presente se hacen inteligibles las sociedades. De allí que, acusiados por nuestro presente, proponemos seguir el hilo de las experiencias, tanteos, controversias y conflictos a través de los cuales la sociedad buscó encontrar su forma legítima. Lo hacemos abordando distintos sub-temas del período, para conocer el modo en que los individuos y los grupos, elaborando su comprensión de las situaciones, rechazaron, adhirieron y formularon sus objetivos a partir de los cuales se propusieron estrategias y organizaron sus acciones. Uno de nuestros más ambiciosos objetivos es conformar un equipo integrado con recursos humanos nuevos y en formación participando en una investigación destinada a rescatar el pasado histórico provincial reciente, cuya realidad se impone conocer dado el papel preponderante desempeñado por Córdoba como condicionante del acaecer nacional.